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Historical Geology/Other isochron methods

In this article I shall point out some other dating methods which work the same way as the Rb-Sr method. The reader who has not read the article on the Rb-Sr method will find this present article almost completely incomprehensible, and should go back and read it.

I have introduced the isochron method in the context of rubidium and strontium. But is there anything particularly special about those two elements? Not really. For the isochron method to work, what we need are three isotopes with the following properties.

(1) An unstableisotope. This should have a fairly long half-life if it is to be of any use in dating rocks, but not too long, or it will hardly undergo any decay at all. A figure expressible in billions of years is ideal. In the Rb-Sr method, we used 87Rb.

The table below shows some sets of three isotopes which can be treated like rubidium and strontium for the purposes of dating; the table also shows the half-life of the parent and its decay mode. The numbers (1) (2) and (3) are as in the section above.

I said that isotope (3) should be stable. 186Os is not in fact stable, but as it has a half-life of two quadrillion years, it might as well be.

In the Lu-Hf method, again, 144Nd is unstable, but has a half-life even longer than that of 186Os.

Similarly in the La-Ce method, neitherisotope of cerium used is strictly speaking stable, but their half-lives are so enormously long that for all practical purposes they may be treated as stable.

In using the K-Ca method, we have to make a slight mathematical adjustment to take into account the fact, mentioned in our article on the K-Ar method, that 40K decays to 40Ar as well as to 40Ca.

Similarly, 138La can decay two ways, to 138Ce or 138Ba. As you can see from the table, both are susceptible to the isochron method.

We have noted the peculiarities of the half-life of 187Re in the article on radioactive decay. As we only have to consider how it behaves in rocks, and not in elaborate equipment in physics laboratories, we may take its half-life to be 43 billion years as given in the table.

There are two entries for U-Pb because there are two parent isotopes we can use, 238U and 235U. Each decays to a (different) final stable element of lead by a complex decay chain.

In practice, the U-Pb decay chain is usually exploited by methods other than isochron dating, for reasons that will be explained in the next article.